Geology of the Comayagua Quadrangle, Honduras, Central America
The Montaña de Comayagua structural belt is a zone trending N. 60° W., more than 130 kilometers long, of exposed earliest Tertiary and older rocks that were complexly deformed during the Laramide orogeny. The Honduras Depression, a discontinuous north-trending graben system, extends from the Pacifi...
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| Format: | Others |
| Language: | English |
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2014
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| Online Access: | http://hdl.handle.net/2152/25301 |